served from IRI/LDEO Climate Data Library
IGOSS leetma d20C: Depth of 20C data
Depth of 20C from IGOSS leetma: Pacific surface currents and equatorial thermocline depth.Independent Variables (Grids)
- Time
- grid: /T (months since 1960-01-01) ordered (Jan 1980) to (Oct 2008) by 1.0 N= 346 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) ordered (122.25E) to (71.25W) by 1.5 N= 112 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (35S) to (45N) by 1.0 N= 81 pts :grid
Other Info
- CE
- 200
- CS
- 0
- datatype
- realarraytype
- gridid
- 189318480
- maxncolor
- 254
- missing_value
- NaN
- positive
- down
- scale_max
- 200.0
- scale_min
- 0.0
- units
- m
- standard units*
- meter
- history
- toS: regridded Z to NOAA NCEP EMC CMB Pacific monthly temp
- colorscale
Last updated: Mon, 12 Sep 2016 21:30:55 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts| T | X | Y | |
 IGOSS leetma d20C[ X Y T |] | M | M | M |
|---|
Filters
Here are some filters that are useful for manipulating data. There are actually many more available, but they have to be entered manually. See Ingrid Function Documentation for more information.- Monthly Climatology calculates a monthly climatology by averaging over all years.
- anomalies calculates the difference between the (above) monthly climatology and the original data.
- Integrate along X Y T
- Differentiate along X Y T
- Take differences along X Y T
RMS (root mean square with mean *not* removed) over X Y T | X Y X T Y T | X Y T |
RMSA (root mean square with mean removed) over X Y T | X Y X T Y T | X Y T |
Maximum over X Y T | X Y X T Y T | X Y T |
Minimum over X Y T | X Y X T Y T | X Y T |
Detrend (best-fit-line) over X Y T | X Y X T Y T | X Y T |
Note on units